This book looks at the sedimentation of the organic material found in sedimentary rocks.
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Microscopic organic-walled fossils are found in most sedimentary rocks. The organic particles - spores, pollens and other land and marine derived microfossils, representing animals, plants, fungi and protists - can be extracted and used to date the rock, reveal details of the original sedimentary environment and provide information on the climate of the time. The mix within a sediment of whole organic particles - palynomorphs - and organic fragments - palynodebris - form palynofacies. This book presents research work on the sedimentation of components of palynofacies and details their importance for sequence stratigraphy and the interpretation of ancient biologic and geologic environments. A comprehensive introduction to the subject is presented in the first chapter. Palynosedimentation in modern environments, the reconstruction of terrestrial vegetation and the application of the data to sequence stratigraphy are then considered. Later chapters detail various quantitative methods and their specific applications in the subject. This is a valuable reference work for palynologists and sedimentologists and also for paleobiologists, and for professionals working in the hydrocarbons industries.
'In summary, this is a very valuable volume which should be available to all palaeopalynologists.' J. E. A. Marshall, Cretaceous Research
' ... obligatory for libraries of universities, consultancy companies as well as the industry related to oil exploration. The book is very well produced, has high quality illustrations ... Prof. Alfred Traverse is to be congratulated on having found so many palynologists willing to contribute to this monumental volume.' Earth Science Reviews
'All postgraduate, academic and other professional palynologists ought to find something of interest in this volume.' Geoscientist
Les informations fournies dans la section « A propos du livre » peuvent faire référence à une autre édition de ce titre.
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Paperback. Etat : new. Paperback. Microscopic organic-walled fossils are found in most sedimentary rocks. The organic particles - spores, pollens and other land and marine derived microfossils, representing animals, plants, fungi and protists - can be extracted and used to date the rock, reveal details of the original sedimentary environment and provide information on the climate of the time. The mix within a sediment of whole organic particles - palynomorphs - and organic fragments - palynodebris - form palynofacies. This book presents research work on the sedimentation of components of palynofacies and details their importance for sequence stratigraphy and the interpretation of ancient biologic and geologic environments. A comprehensive introduction to the subject is presented in the first chapter. Palynosedimentation in modern environments, the reconstruction of terrestrial vegetation and the application of the data to sequence stratigraphy are then considered. Later chapters detail various quantitative methods and their specific applications in the subject. This is a valuable reference work for palynologists and sedimentologists and also for paleobiologists, and for professionals working in the hydrocarbons industries. This book deals with the sedimentation of the organic material found in sedimentary rocks. A valuable reference work for palynologists, sedimentologists, paleobiologists, and for professionals working in the hydrocarbons industries. This item is printed on demand. Shipping may be from multiple locations in the US or from the UK, depending on stock availability. N° de réf. du vendeur 9780521675505
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Etat : New. This book looks at the sedimentation of the organic material found in sedimentary rocks. Editor(s): Traverse, Alfred. Num Pages: 560 pages, 258 b/w illus. 68 tables. BIC Classification: RBGG. Category: (P) Professional & Vocational. Dimension: 276 x 219 x 29. Weight in Grams: 1250. . 2005. Revised ed. paperback. . . . . N° de réf. du vendeur V9780521675505
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